Research note: Laboratory study of the influence of changing the injection rate on the geometry of the fluid front and on P‐wave ultrasonic velocities in sandstone |
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Authors: | Sofia Lopes Maxim Lebedev |
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Affiliation: | 1. Department of Exploration Geophysics, Curtin University, GPO Box U1987, 6845 Perth, Western Australia, Australia;2. CSIRO, Earth Science and Resource Engineering, 26 Dick Perry Avenue, 6151 Kensington, Western Australia, Australia;3. CO2CRC, Department of Exploration Geophysics, Curtin University, GPO Box U1987, 6845 Perth, Western Australia, Australia |
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Abstract: | Forced imbibition was performed in reservoir sandstone by injecting water into a dry sample. The injection was monitored with X‐ray computed tomography and acoustic acquisition to simultaneously visualize the displacement of the fluid and quantify its presence by calculating saturation and P‐wave velocities. We observed a strong influence when changing the injection rates on the acoustic response. Upon decreasing the injection rate from 5 mL/h to 0.1 mL/h, P‐wave velocities decreased sharply: 100 m/s in 1 h. This behaviour is related to the partially saturated conditions of the sample (76% of saturation) before decreasing the injection rate. The air that is still trapped is free to move due to a decrease of pore pressure that is no longer forced by the higher injection rate. After 1 hour, P‐wave velocities started increasing with small changes in saturation. Stopping injection for 16 hrs decreased saturation by 8% and P‐wave velocities by 100 m/s. Restarting injection at 5 mL/h increased saturation to 76% while P‐wave velocities fluctuated considerably for 2 hrs until they stabilized at 2253 m/s. Through the computed tomography scans we observed a water front advancing through the sample and how its shape changed from a plane to a curve after decreasing the injection rate. |
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Keywords: | Injection rate Imbibition |
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